CIFOR-ICRAF berfokus pada tantangan-tantangan dan peluang lokal dalam memberikan solusi global untuk hutan, bentang alam, masyarakat, dan Bumi kita

Kami menyediakan bukti-bukti serta solusi untuk mentransformasikan bagaimana lahan dimanfaatkan dan makanan diproduksi: melindungi dan memperbaiki ekosistem, merespons iklim global, malnutrisi, keanekaragaman hayati dan krisis disertifikasi. Ringkasnya, kami berupaya untuk mendukung kehidupan yang lebih baik.

Découvrez les évènements passés et à venir dans le monde entier et en ligne, qu’ils soient organisés par le CIFOR-ICRAF ou auxquels participent nos chercheurs.

CIFOR-ICRAF menerbitkan lebih dari 750 publikasi setiap tahunnya mengenai agroforestri, hutan dan perubahan iklim, restorasi bentang alam, pemenuhan hak-hak, kebijakan hutan dan masih banyak lagi – juga tersedia dalam berbagai bahasa..

CIFOR-ICRAF berfokus pada tantangan-tantangan dan peluang lokal dalam memberikan solusi global untuk hutan, bentang alam, masyarakat, dan Bumi kita

Kami menyediakan bukti-bukti serta solusi untuk mentransformasikan bagaimana lahan dimanfaatkan dan makanan diproduksi: melindungi dan memperbaiki ekosistem, merespons iklim global, malnutrisi, keanekaragaman hayati dan krisis disertifikasi. Ringkasnya, kami berupaya untuk mendukung kehidupan yang lebih baik.

CIFOR–ICRAF publishes over 750 publications every year on agroforestry, forests and climate change, landscape restoration, rights, forest policy and much more – in multiple languages.

CIFOR–ICRAF addresses local challenges and opportunities while providing solutions to global problems for forests, landscapes, people and the planet.

We deliver actionable evidence and solutions to transform how land is used and how food is produced: conserving and restoring ecosystems, responding to the global climate, malnutrition, biodiversity and desertification crises. In short, improving people’s lives.

Soil organic matter stabilization and associated degradation threshold dynamics

Ekspor kutipan

Models that describe Soil Organic Carbon (SOC) dynamics ignore functional relationships that occur during land use which may confer degradation thresholds. We investigated the dynamics of soil organic matter degradation on an Oxisol following conversion of native forest vegetation to agriculture along a 100 year cultivation chronosequence in western Kenya. Seven broad categories of agricultural conversion sites were identified, representing < 3, 3-9, 10-22, 23-34, 35-57, 58-83 and > 83 years following cultivation. Soil samples were collected from randomly selected agricultural fields where maize was historically cultivated with little or no fertilizer/manure inputs. Twelve undisturbed forest reference plots were included in a paired combination with the cultivated plots. Soil samples were treated to a two step organic matter fractionation process involving density separation with sodium iodide and physical energy disruption through sonication to yield three functional organic C pools that were related to seasonal C dynamics, aggregate C protection and long-term soil C stabilization. The pools were sequentially separated from soil as light-fraction C, recovered following density flotation at 1.8 g cm-3, aggregate-protected C, isolated after density separation following high energy sonication and organo-mineral associated C from the residue. Mass spectrometry evaluations of 13C signature were used to partition resident C stocks into native forest C3 C and contemporary C4 crop C sources. SOC declined rapidly and reached a new equilibrium beyond 40 years of maize cultivation at which time the soil C (19 g C kg-1) and N (2.0 g kg-1) contents were less than 20% of the original forest C (101 g C kg-1) and N (25.3 g kg-1). At this new stable equilibrium point, the 13 C values revealed that one half of the remaining C is of C3 native forest origin while the other half is due to C4 cultivated crop inputs. In addition, biogeochemical transformations of C and N within functionally specific fractions will be reported.

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